A B C D E F G H I J K L M N O P Q R S T U V W X Y Z All
Joshi, Mallickarjun
- Neotectonic Movements in the Loharkhet Area, District Almora, Kumann Fiimalaya
Authors
1 Department of Geology, Kumaun University, Nainital 263 002, IN
2 Department of Civil Engg., Institute of Technology, BHU, Varanasi 221005, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 39, No 3 (1992), Pagination: 245-253Abstract
Thrusts, fold axes and fault zones in the Loharkhet area in the northern part of Almora district in Uttar Pradesh, record reactivation during Neogene times. Several alluvial and colluvial deposits in the area are being vertically and horizontally offset, and tilted by active folding and faulting. The recent movements along the Ravetiganga overturned anticline and Dulam Gadhera- and Vongarh-Gason-faults have not only uplifted the Nasati-Rithabagar block by about 103 m, but have shifted also the original confluence of the Sarju and Ravetiganga rivers by 11 km southwestward.
The ESE-flowing Gurkhula Gad and Mehar Gad streams have been deflected towards SSE direction by the recent strike-slip movements along the Kaphlikot-Ramari Fault. The Ramari landslides fan has been displaced vertically by 3 m along this fault. Terraced toe of the colluvial cone of the Badiyakot landslide has been displaced dextrally and uplifted by 18 m along the NNW-SSE striking Ghatia Gad Fauh.
The geomorphic expressions of the various tectonic zones indicate both vertical and strike-slip displacements. Rejuvenation of the earlier mature terrain is borne out by topographic changes that have taken place in the recent past. The topographic development indicates continuing uplift in some sections of Vaikrita (MC) Thrust and Berinag Thrust and the zone of the Ravetiganga overturned anticline. Relatively higher rate of uplift is observed for the MCT zone.
Keywords
Neotectonism, Geomorphology, Kumaun Himalaya.- Geochemistry and Petrogenesis of the Champawat Granitoids Occurring around Dhunaghat, District Pithoragarh, Uttar Pradesh, India
Authors
1 Department of Geology, Kumaun University, Nainital 263 002, IN
2 Geology Laboratory, Department of Civil Engineering, Institute of Technology, Banaras University, Varanasi-221 005, IN
3 Australian Geological Survey Organisation, P. O. Box 378, Canberra City, A.C.T. 2601, AU
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 42, No 3 (1993), Pagination: 289-302Abstract
Early Cambrian Champawat granitoids from Dhunaghat area, emplaced between medium-to high-grade metapelites of the Saryu Formation and low-grade melapelites of the Gumalikhet Formation of the Almora Group, show wide variations in their modal and chemical composition, ranging from granodiorite to granite. Biotite-rich mafic enclaves within the granitoids may represent restile, possibly modified by metasomatism. Chemical data for the calc-alkaline Champwat granitoids show some dcgree of fractional crystallization, although processes such as restite unmixing and different degree of melting may also have been important for the observed variation trends.
The Champwat intrusives are also characterized by enrichment of Y, Zr, Th, U, Nb, La, Ce, Pr and Nd and show affinities with "A"-type (anorogenic) granites.
Keywords
Geochemistry, Petrogenesis, Champawat graniloids, Almora Group, Dhunaghat, District Pithoragarh, Uttar Pradesh.- Geochemistry and Origin of the Granite Gneisses of the Almora Group from Dhunaghat area, District Pithoragarh, U.P.
Authors
1 Geology Laboratory, Department of Civil Engineering, Institute of Technology, Banaras Hindu University, Varanasi - 221 005 (India), IN
2 Department of Geology, Kumaun University, Nainital - 263 002 (India), IN
3 Australian Geological Survey Organisation, P.O. Box 378, Canberra City, A.C.T. 2601 (Australia), AU
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 46, No 1 (1995), Pagination: 27-36Abstract
The Precambrian Almora granite gneisses containing numerous schistose enclaves occuras thick and thin bands within the medium-grade Saryu metasediments of Almora Group. Petrography and major and trace element geochemistry of the granite gneisses indicate that they are strongly peraluminous, S-type granites, and were derived by partial meltingofthe meta-arkose/metapelites.Keywords
Geochemistry, Granite, Dhunaghat, Uttar Pradesh.- Occurrence of Rhyolitic Dykes within the Mt. Abu Batholith, Southwestern Rajasthan
Authors
1 Geology Laboratory, Department of Civil Engineering, Institute of Technology, Banaras Hindu University, Varanasi- 221 005, IN
2 Department of Geology, Banaras Hindu University, Varanasi - 221 005, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 65, No 3 (2005), Pagination: 309-316Abstract
The occurrence of Malani rhyolites as dykes within the Mt. Abu batholith has been studied. The Mt. Abu rhyolitic dykes are peraluminous and of subalkaline nature. These are enriched in trace elements such as Rb, Nb, Zr, Y, Ga, Th and Zn, and depleted in Ba and Sr resulting in high K/Rb, Rb/Sr, Ba/Sr and Ga/AI ratios. The geochemical characters indicate Mt. Abu rhyoiitic dykes to be A-Type, within-Plate granites (WPG) with high SiO2, Na2O + K2O and Fe/Mg. These rhyolites are likely to have formed in anorogenic Rift-Related setting and the volcanism may be correlated to early stages of Pan-African magmatic event (850-750 Ma).Keywords
Rhyolite, Geochemistry, Mt. Abu Batholith, Rajasthan.- Fractal Dimension as a New Measure of Neotectonic Activity in Kakrighat Area, Kumaun Himalaya
Authors
1 Department of Geology, Banaras Hindu University, Varanasi - 221 005, U.P., IN
2 Department of Civil Engineering, Banaras Hindu University, Varanasi - 221 005, U.P., IN